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  • Results for
    • Geological Fold
  • (58)
Geologic folding, Digges Island, Hudson Bay, Canada  -  Tui De Roy
00142100
00142100 Geologic folding, Digges Island, Hudson Bay, Canada© Tui De Roy
Folded ridges, Northern Territory, Australia
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00556785 Folded ridges, Northern Territory, Australia© Colin Monteath/ Hedgehog House
Folded ridges, Northern Territory, Australia
00556781
00556781 Folded ridges, Northern Territory, Australia© Colin Monteath/ Hedgehog House
Folded ridges, Northern Territory, Australia
00556780
00556780 Folded ridges, Northern Territory, Australia© Colin Monteath/ Hedgehog House
Folded ridges, Northern Territory, Australia
00556779
00556779 Folded ridges, Northern Territory, Australia© Colin Monteath/ Hedgehog House
Sedimentary deposit of folded flysch, Alps, France
00566665
00566665 Sedimentary deposit of folded flysch, Alps, France© Jean-Philippe Delobelle/ Biosphoto
Folded rocks on beach with cliffs above. Sandstone and shale beds in Bude Formation. Bude, Cornwall, England, UK. August 2018
90820731
90820731 Folded rocks on beach with cliffs above. Sandstone and shale beds in Bude Formation. Bude, Cornwall, England, UK. August 2018© Mike Read
Wave-cut platform on beach. Folded sandstone and shale beds of Bude Formation. Bude, Cornwall, England, UK. August 2018.
90820728
90820728 Wave-cut platform on beach. Folded sandstone and shale beds of Bude Formation. Bude, Cornwall, England, UK. August 2018.© Mike Read
Banding and folding of rock on cliff above Cyclone Creek. Talbot Bay, The Kimberley, Western Australia. 2015.
90820631
90820631 Banding and folding of rock on cliff above Cyclone Creek. Talbot Bay, The Kimberley, Western Australia. 2015.© Rick Price
Banded and folded rock on cliff beside Cyclone Creek. Talbot Bay, The Kimberley, Western Australia.
90820629
90820629 Banded and folded rock on cliff beside Cyclone Creek. Talbot Bay, The Kimberley, Western Australia.© Rick Price
Conjugate kink bands in Carboniferous turbidite shales, Bude, Cornwall, UK, May
90795868
90795868 Conjugate kink bands in Carboniferous turbidite shales, Bude, Cornwall, UK, May© Graham Eaton
An anticline in deformed Carboniferous sandstones and shale (Culm Measures) near Bude, Cornwall, UK, March. These rocks were deformed during the Hercynian or Variscan Orogeny, a mountain building even...
90795867
90795867 An anticline in deformed Carboniferous sandstones and shale (Culm Measures) near Bude, Cornwall, UK, March. These rocks were deformed during the Hercynian or Variscan Orogeny, a mountain building even...© Graham Eaton
A box fold formed by intersecting kink folds in Carboniferous age Sandstones and Shales (Culm Measures) at Menanchrurch near Bude, Cornwall, March. The deformation of the rocks formed during the Varis...
90795825
90795825 A box fold formed by intersecting kink folds in Carboniferous age Sandstones and Shales (Culm Measures) at Menanchrurch near Bude, Cornwall, March. The deformation of the rocks formed during the Varis...© Graham Eaton
Chevron folded Carboniferous age sandstone and shale (Culm Measures), deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Late Paleozoic cont...
90795824
90795824 Chevron folded Carboniferous age sandstone and shale (Culm Measures), deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Late Paleozoic cont...© Graham Eaton
A monocline fold with a minor thrust fault in Carboniferous age sandstones, Bude, Cornwall, UK, May.
90795816
90795816 A monocline fold with a minor thrust fault in Carboniferous age sandstones, Bude, Cornwall, UK, May.© Graham Eaton
Chevron recumbent foldeding in Carboniferous age sandstone and shale (Culm Measures), deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Lat...
90795810
90795810 Chevron recumbent foldeding in Carboniferous age sandstone and shale (Culm Measures), deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Lat...© Graham Eaton
Chevron recumbent foldeding in Carboniferous age sandstone and shale (Culm Measures), deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Lat...
90795809
90795809 Chevron recumbent foldeding in Carboniferous age sandstone and shale (Culm Measures), deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Lat...© Graham Eaton
Recumbent folds in Carboniferous age sandstones and Shale (Bude Formation), Bude, Cornwall, UK, May. The rocks were deformed during the Hercynian Orogeny or mountain building event.
90795808
90795808 Recumbent folds in Carboniferous age sandstones and Shale (Bude Formation), Bude, Cornwall, UK, May. The rocks were deformed during the Hercynian Orogeny or mountain building event.© Graham Eaton
Recumbent folds in Carboniferous age sandstones and Shale (Bude Formation), Bude, Cornwall, UK, May. The rocks were deformed during the Hercynian Orogeny or mountain building event.
90795807
90795807 Recumbent folds in Carboniferous age sandstones and Shale (Bude Formation), Bude, Cornwall, UK, May. The rocks were deformed during the Hercynian Orogeny or mountain building event.© Graham Eaton
Small Waterfalls at Sandy Mouth beach, near Bude, Cornwall, UK, March. The rocks are steeply dipping Carboniferous age, sandstone and shale (Culm Measures).
90795805
90795805 Small Waterfalls at Sandy Mouth beach, near Bude, Cornwall, UK, March. The rocks are steeply dipping Carboniferous age, sandstone and shale (Culm Measures).© Graham Eaton
A small waterfall at Sandy Mouth beach, near Bude, Cornwall, UK, March. The rocks are steeply dipping Carboniferous age, sandstone and shale (Culm Measures).
90795804
90795804 A small waterfall at Sandy Mouth beach, near Bude, Cornwall, UK, March. The rocks are steeply dipping Carboniferous age, sandstone and shale (Culm Measures).© Graham Eaton
Quartz infilled tension cracks in a boulder on the beach. Millock Haven, Cornwall, UK, March
90795796
90795796 Quartz infilled tension cracks in a boulder on the beach. Millock Haven, Cornwall, UK, March© Graham Eaton
A thrust fault in Carboniferous age Sandstones and shales (Culm Measures) at Crackington Haven, near Bude, Cornwall, March. The rocks comprise the Crackington Formation of thinly bedded turbidite sand...
90795792
90795792 A thrust fault in Carboniferous age Sandstones and shales (Culm Measures) at Crackington Haven, near Bude, Cornwall, March. The rocks comprise the Crackington Formation of thinly bedded turbidite sand...© Graham Eaton
A thrust fault in Carboniferous age Sandstones and shales (Culm Measures) at Crackington Haven, near Bude, Cornwall, March. The rocks comprise the Crackington Formation of thinly bedded turbidite sand...
90795791
90795791 A thrust fault in Carboniferous age Sandstones and shales (Culm Measures) at Crackington Haven, near Bude, Cornwall, March. The rocks comprise the Crackington Formation of thinly bedded turbidite sand...© Graham Eaton
A small relay thrust fault in steeply dipping Carboniferous age Sandstones and shales (Culm Measures) near Bude, Cornwall, March.
90795790
90795790 A small relay thrust fault in steeply dipping Carboniferous age Sandstones and shales (Culm Measures) near Bude, Cornwall, March.© Graham Eaton
An anticlinal fold in Carboniferous age sandstone and shales. This angular anticline is a kink fold with a defined fracture along the fold axis. These rocks were folded and faulted during the Variscan...
90795786
90795786 An anticlinal fold in Carboniferous age sandstone and shales. This angular anticline is a kink fold with a defined fracture along the fold axis. These rocks were folded and faulted during the Variscan...© Graham Eaton
Steeply dipping beds of Carboniferous age sandstone and shales (Culm measures) on the flank of a large fold. This deformation was formed by compression during the Variscan or Hercynian orogeny, a geol...
90795784
90795784 Steeply dipping beds of Carboniferous age sandstone and shales (Culm measures) on the flank of a large fold. This deformation was formed by compression during the Variscan or Hercynian orogeny, a geol...© Graham Eaton
Tilted beds of sandstone and thin shales of the Carboniferous, Culm Measures (Bude Formation) Sandy Mouth near Bude, Cornwall, UK, May. The bed represent cycles of deposition associated with climate c...
90795783
90795783 Tilted beds of sandstone and thin shales of the Carboniferous, Culm Measures (Bude Formation) Sandy Mouth near Bude, Cornwall, UK, May. The bed represent cycles of deposition associated with climate c...© Graham Eaton
Tilted beds of Carboniferous age, Culm Measures (Bude Formation) sandstone and shale, Bude, Cornwall, UK, May.
90795782
90795782 Tilted beds of Carboniferous age, Culm Measures (Bude Formation) sandstone and shale, Bude, Cornwall, UK, May.© Graham Eaton
A Chevron or Kink fold anticline in Carboniferous age turbidite sediments. Bude, Cornwall, UK, may.
90795781
90795781 A Chevron or Kink fold anticline in Carboniferous age turbidite sediments. Bude, Cornwall, UK, may.© Graham Eaton
Tilted beds of sandstone and thin shales of the Carboniferous, Culm Measures (Bude Formation) Sandy Mouth near Bude, Cornwall, UK, May. The bed represent cycles of deposition associated with climate c...
90795776
90795776 Tilted beds of sandstone and thin shales of the Carboniferous, Culm Measures (Bude Formation) Sandy Mouth near Bude, Cornwall, UK, May. The bed represent cycles of deposition associated with climate c...© Graham Eaton
Folded Carboniferous age sandstone and shale (Culm Measures) in plan view, deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Late Paleozoic...
90795775
90795775 Folded Carboniferous age sandstone and shale (Culm Measures) in plan view, deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Late Paleozoic...© Graham Eaton
Small extension (normal) faults within a layer of shale between two layers of more competent sandstone. Carboniferous, turbidites, Bude, Cornwall, UK, May.
90795771
90795771 Small extension (normal) faults within a layer of shale between two layers of more competent sandstone. Carboniferous, turbidites, Bude, Cornwall, UK, May.© Graham Eaton
Folded Carboniferous age sandstone and shale (Culm Measures) in plan view, deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Late Paleozoic...
90795768
90795768 Folded Carboniferous age sandstone and shale (Culm Measures) in plan view, deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Late Paleozoic...© Graham Eaton
An anticlinal fold in Carboniferous age sandstone and shales. This fold and deformation was formed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by...
90795767
90795767 An anticlinal fold in Carboniferous age sandstone and shales. This fold and deformation was formed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by...© Graham Eaton
Folded Carboniferous age sandstone and shale (Culm Measures) deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Late Paleozoic continental c...
90795759
90795759 Folded Carboniferous age sandstone and shale (Culm Measures) deformed by compression during the Variscan or Hercynian orogeny, a geologic mountain-building event caused by Late Paleozoic continental c...© Graham Eaton
Monocline fold that has been faulted during the Variscan orogeny, in Carboniferous sandstone and shale. Broad Haven, Pembrokeshire, Wales, UK, May
90773222
90773222 Monocline fold that has been faulted during the Variscan orogeny, in Carboniferous sandstone and shale. Broad Haven, Pembrokeshire, Wales, UK, May© Graham Eaton
A monocline fold that has been faulted during the Variscan orogeny, in Carboniferous sandstone and shale. Broad Haven, Pembrokeshire, Wales, UK, May
90773221
90773221 A monocline fold that has been faulted during the Variscan orogeny, in Carboniferous sandstone and shale. Broad Haven, Pembrokeshire, Wales, UK, May© Graham Eaton
Sea cliffs, geological section through Cambrian and Ordovician sedimentary rocks with faulted monocline fold structure. Rocks include Nant-pig Musdstones, Abersoch, Gwynedd,  Wales, UK
90768424
90768424 Sea cliffs, geological section through Cambrian and Ordovician sedimentary rocks with faulted monocline fold structure. Rocks include Nant-pig Musdstones, Abersoch, Gwynedd, Wales, UK© Graham Eaton
Cilan Headland, a headland of folded and tilted Cambrian and Ordovician age sedimentary rocks, Abersoch, Gwynedd, Wales, UK, August 2016.
90768423
90768423 Cilan Headland, a headland of folded and tilted Cambrian and Ordovician age sedimentary rocks, Abersoch, Gwynedd, Wales, UK, August 2016.© Graham Eaton
Steeply dipping beds of Silurian age turbidite sediments, Clarach Bay, Aberystwyth, Wales, UK, September 2014.
90768422
90768422 Steeply dipping beds of Silurian age turbidite sediments, Clarach Bay, Aberystwyth, Wales, UK, September 2014.© Graham Eaton
Harpea's Cave, limestone cave is an example of anticline folding, Pyrenees, France
00595105
00595105 Harpea's Cave, limestone cave is an example of anticline folding, Pyrenees, France© Georges Lopez/ Biosphoto
The Rock of Falize, a Frasnian limestone anticline (convex geological fold) from the Devonian era Durbuy, Belgium  -  Philippe Clement/ npl
90348209
90348209 The Rock of Falize, a Frasnian limestone anticline (convex geological fold) from the Devonian era Durbuy, Belgium© Philippe Clement / NPL
The Rock of Falize, a Frasnian limestone anticline (convex geological fold) from the Devonian era Durbuy, Belgium  -  Philippe Clement/ npl
90348178
90348178 The Rock of Falize, a Frasnian limestone anticline (convex geological fold) from the Devonian era Durbuy, Belgium© Philippe Clement / NPL
Synclinal chevron fold in Silurian mudstones, on the grassy plateau beyond can be seen the remains of an Iron Age fort 'Castell Bach', Cerediogion, West Wales, UK  -  Sinclair Stammers/ npl
90110664
90110664 Synclinal chevron fold in Silurian mudstones, on the grassy plateau beyond can be seen the remains of an Iron Age fort 'Castell Bach', Cerediogion, West Wales, UK© SINCLAIR STAMMERS / NPL
Quarry face showing strongly folded Ystrad Meurig Grits Formation of early Silurian age, Ystrad Meurig Quarry, Ceredigion, Wales, April  -  Richard Becker / FLPA
80190126
80190126 Quarry face showing strongly folded Ystrad Meurig Grits Formation of early Silurian age, Ystrad Meurig Quarry, Ceredigion, Wales, April© Richard Becker / FLPA
View of coastline with heavily folded sandstone and mudstone rocks, Hartland Quay, North Devon, England, may  -  Bob Gibbons/ FLPA
80142672
80142672 View of coastline with heavily folded sandstone and mudstone rocks, Hartland Quay, North Devon, England, may© Bob Gibbons / FLPA
Heavily folded sandstone and mudstone rocks with surf, Hartland Quay, North Devon, England, may  -  Bob Gibbons/ FLPA
80142671
80142671 Heavily folded sandstone and mudstone rocks with surf, Hartland Quay, North Devon, England, may© Bob Gibbons / FLPA
Heavily folded sandstone and mudstone rocks, Hartland Quay, North Devon, England, may  -  Bob Gibbons/ FLPA
80142670
80142670 Heavily folded sandstone and mudstone rocks, Hartland Quay, North Devon, England, may© Bob Gibbons / FLPA
Geological site with information sign, folded Cretaceous Middle Chalk formations, Steeple Pit, Dorset, England, april  -  Nicholas and Sherry Lu Aldridge/
80101322
80101322 Geological site with information sign, folded Cretaceous Middle Chalk formations, Steeple Pit, Dorset, England, april© Nicholas and Sherry Lu Aldridge / FLPA
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